Articles | Volume 15, issue 21
https://doi.org/10.5194/amt-15-6387-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-15-6387-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Long-distance propagation of 162 MHz shipping information links associated with sporadic E
Alex T. Chartier
CORRESPONDING AUTHOR
Space Exploration Sector, Johns Hopkins University Applied Physics Laboratory, Laurel, MD
20723, United States of America
Thomas R. Hanley
Space Exploration Sector, Johns Hopkins University Applied Physics Laboratory, Laurel, MD
20723, United States of America
Daniel J. Emmons
Air Force Institute of Technology, Wright-Patterson AFB, OH 45433,
United States of America
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We studied how the 2021 total solar eclipse over Antarctica affected the upper atmosphere near the South Pole. Using HF radars, we observed changes in radio wave behavior and fast plasma flows in the ionosphere, including sudden high-velocity echoes that tracked the eclipse shadow. Satellite data and models revealed changes in ionospheric currents and conductance. These findings show eclipses can temporarily reshape magnetosphere-ionosphere interactions at polar latitudes.
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Sub-auroral polarisation streams (SAPSs) are very fast plasma flows that occur at mid-latitudes, which can affect the atmosphere. In this paper, we use four ground-based radars to obtain a wide coverage of SAPSs that occurred over the USA, along with interferometer cameras in Virginia and Massachusetts to measure winds. The winds are strongly affected but in different ways, implying that the balance forces on the atmosphere is strongly dependent on proximity to the disturbance.
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Short summary
This is a study of anomalous long-distance (>1000 km) radio propagation that was identified in United States Coast Guard monitors of automatic identification system (AIS) shipping transmissions at 162 MHz. Our results indicate this long-distance propagation is caused by dense sporadic E layers in the daytime ionosphere, which were observed by nearby ionosondes at the same time. This finding is surprising because it indicates these sporadic E layers may be far more dense than previously thought.
This is a study of anomalous long-distance (1000 km) radio propagation that was identified in...